978 resultados para fertilizer 15N
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Different problems are daily discuss on environmental aspects such acid rain, eutrophication, global warming and an others problems. Rarely do we find some discussions about phosphorus problematic. Through the years the phosphorus as been a real problem and must be more discussed. On this thesis was done a global material flow analysis of phosphorus, based on data from the year 2004, the production of phosphate rock in that year was 18.9 million tones, almost this amount it was used as fertilizer on the soil and the plants only can uptake, on average, 20% of the input of fertilizer to grow up, the remainder is lost for the phosphorus soil. In the phosphorus soil there is equilibrium between the phosphorus available to uptake from the plants and the phosphorus associate with other compounds, this equilibrium depends of the kind of soil and is related with the soil pH. A reserve inventory was done and we have 15,000 million tones as reserve, the amount that is economical available. The reserve base is estimated in 47,000 million tones. The major reserves can be found in Morocco and Western Sahara, United Sates, China and South Africa. The reserve estimated in 2009 was 15,000 million tone of phosphate rock or 1,963 million tone of P. If every year the mined phosphate rock is around 22 Mt/yr (phosphorus production on 2008 USGS 2009), and each year the consumption of phosphorus increases because of the food demand, the reserves of phosphate rock will be finished in about 90 years, or maybe even less. About the value/impact assessment was done a qualitative analysis, if on the future we don’t have more phosphate rock to produce fertilizers, it is expected a drop on the crops yields, each depends of the kind of the soil and the impact on the humans feed and animal production will not be a relevant problem. We can recovery phosphorus from different waste streams such as ploughing crop residues back into the soil, Food processing plants and food retailers, Human and animal excreta, Meat and bone meal, Manure fibre, Sewage sludge and wastewater. Some of these examples are developed in the paper.
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Trabalho de Dissertação de Natureza Científica para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização em Hidráulica
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Protein Science (2002), 11:2464–2470
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J Biol Inorg Chem (2003) 8: 777–786
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This work evaluates the possibility of using spent coffee grounds (SCG) for biodiesel production and other applications. An experimental study was conducted with different solvents showing that lipid content up to 6 wt% can be obtained from SCG. Results also show that besides biodiesel production, SCG can be used as fertilizer as it is rich in nitrogen, and as solid fuel with higher heating value (HHV) equivalent to some agriculture and wood residues. The extracted lipids were characterized for their properties of acid value, density at 15 °C, viscosity at 40 °C, iodine number, and HHV, which are negatively influenced by water content and solvents used in lipid extraction. Results suggest that for lipids with high free fatty acids (FFA), the best procedure for conversion to biodiesel would be a two-step process of acid esterification followed by alkaline transesterification, instead of a sole step of direct transesterification with acid catalyst. Biodiesel was characterized for its properties of iodine number, acid value, and ester content. Although these quality parameters were not within the limits of NP EN 14214:2009 standard, SCG lipids can be used for biodiesel, blended with higher-quality vegetable oils before transesterification, or the biodiesel produced from SCG can be blended with higher-quality biodiesel or even with fossil diesel, in order to meet the standard requirements.
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Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Biotecnologia
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Dissertação para obtenção do Grau de Mestre em Bioquímica Estrutural e Funcional
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Avaliou-se a capacidade de suprimento de potassio de cinco solos do Submedio Sao Francisco, denominados de Bebedouro 6, Bebedouro 3, Massangano, Mandacaru e Salitre. Os tres primeiros sao classificados como Latossolo Vermelho-Amarelo e os dois ultimos como Vertissolo e Bruno Nao-Calcico, respectivamente. Dois litros de cada solo com e sem adicao de potassio, 1,6 k, foram acondicionados em vasos e submetidos a um cultivo de sorgo e cinco de milho durante nove meses. A parte aerea das plantas foi colhida cinco semanas depois do plantio. A producao total de materia seca (MS) das plantas nos solos que receberam K foi significativamente superior, 37% a 154%, em relacao aquela obtida nos solos sem adicao de K. A MS apresentou correlacoes significativas com o K absorviso pelas plantas (r= 0,98**), com o K do solo nas formas de K-NH4OAC1N (r= 0,95*), e de K-Mehlich pelas plantas (r= 0.89*) e com liberacao e K para as plntas da forma nao trocavel (r= 0.96**) e uma correlacao nao significativa (r= 0.87 ns), com K extraido do solo pelo HNO31N fervente. A capacidade de suprimento de K avaliada pelos cultivos de plantas, foi de 0,23; 0,37; 0,23; 0,32 e 0,56 meq/100 ml para os solos Bebedouro 6, Bebedouro 3, Massangana, Mandacaru e Salitre, respectivamente. O K-NH4OAC1N por ter apresentado tambem uma correlacao altamente significativa (r= 0,99**), com a reserva de K no solo, foi o indice mais util para avaliar a capacidade de suprimento de potassio dos solos estruturados.
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Resumo: Objetivou-se avaliar gramíneas com reconhecida tolerância a períodos de estresse hídrico em consórcio com a cultura do milheto e doses de nitrogênio. O ensaio foi realizado em Sobral-CE, em delineamento em blocos casualizados com os tratamentos sendo o consórcio da cultura do milheto com o capim-buffel ou capim-massai, com 3 doses de adubação em cobertura para o milheto, sendo: 0, 50 e 100 kg ha-1 de nitrogênio, e o tratamento testemunha sendo o plantio do milheto solteiro sem adubação de cobertura; com 3 blocos. Avaliaram-se os dados biométricos e produtividade de massa seca. O consórcio de culturas anuais com gramíneas forrageiras é alternativa interessante para produção de volumoso em região semiárida. O consórcio de milheto e capim-massai mostrou-se superior para dados biométricos e produtividade. O emprego de 100 kg ha-1 de N em cobertura na cultura do milheto propiciou maior produtividade de massa seca. [Millet production with forage consortium in semiarid region of State of Ceará]. Abstract: This study aimed to evaluate grasses with recognized tolerance to periods of water stress in partnership with millet cultivation and doses of nitrogen. The test was conducted in Sobral-CE, at a randomized block with treatments and millet culture consortium with buffel grass or massai grass with 3 fertilizer levels at coverage for millet, as follows: 50 and 100 kg ha-1 of nitrogen, and the control treatment being the planting millet single without cover fertilization; with 3 blocks. Evaluated were the biometric data and dry matter productivity. The consortium of annual crops with grasses is interesting alternative to massive production for semi-arid region. The consortium millet and massai grass was superior to biometric data and productivity. The use of 100 kg ha-1 of N topdressing in the millet culture provided greater dry mass productivity.
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World population is increasing at an alarming rate while food productivity is decreasing due to the effect of various abiotic stresses. Soil salinity is one of the most important abiotic stress and a limiting factor for worldwide plant production. In addition to its important effects on yield, salt stress affects numerous cellular activities, including cell wall composition, photosynthesis, protein synthesis, ions and organic solutes. Up to 20% of the irrigated arable land in arid and semiarid regions is already salt affected and is still expanding. Improving salt tolerant varieties is of major importance, and efforts should be focused on finding adaptive mechanisms which are involved in salinity tolerance. In this study, several spelt wheat (Triticum aestivum var. Spelta) genotypes and one cultivar of modern bread wheat were used to screen them for salt tolerance. Spelt is an old-European cereal crop currently attracting renewed interest as a food grain because it is said to be harder than wheat and requires less fertilizer. Spelt wheat is also becoming very attractive genetic source by plant breeders due to its wide adaptation ability to various stressful conditions such as soil salinity. In this study morphological parameters (e.g., leaf appearance; shoot elongation), dry matter production, mineral nutrients (especially Na and K), and activity of antioxidative enzymes were measured to select superior genotypes of spelt for salt tolerance. The results showed that Spelt genotype Sp41 is a salt sensitive genotype and genotypes Sp69, Sp96 and Sp912 are good candidates for salt tolerant genotypes.
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Phosphorus (P) is becoming a scarce element due to the decreasing availability of primary sources. Therefore, recover P from secondary sources, e.g. waste streams, have become extremely important. Sewage sludge ash (SSA) is a reliable secondary source of P. The use of SSAs as a direct fertilizer has very restricted legislation due to the presence of inorganic contaminants. Furthermore, the P present in SSAs is not in a plant-available form. The electrodialytic (ED) process is one of the methods under development to recover P and simultaneously remove heavy metals. The present work aimed to optimize the P recovery through a 2 compartment electrodialytic cell. The research was divided in three independent phases. In the first phase, ED experiments were carried out for two SSAs from different seasons, varying the duration of the ED process (2, 4, 6 and 9 days). During the ED treatment the SSA was suspended in distilled water in the anolyte, which was separated from the catholyte by a cation exchange membrane. From both ashes 90% of P was successfully extracted after 6 days of treatment. Regarding the heavy metals removal, one of the SSAs had a better removal than the other. Therefore, it was possible to conclude that SSAs from different seasons can be submitted to ED process under the same parameters. In the second phase, the two SSAs were exposed to humidity and air prior to ED, in order to carbonate them. Although this procedure was not successful, ED experiments were carried out varying the duration of the treatment (2 and 6 days) and the period of air exposure that SSAs were submitted to (7, 14 and 30 days). After 6 days of treatment and 30 days of air exposure, 90% of phosphorus was successfully extracted from both ashes. No differences were identified between carbonated and non-carbonated SSAs. Thus, SSAs that were exposed to the air and humidity, e.g. SSAs stored for 30 days in an open deposit, can be treated under the same parameters as the SSAs directly collected from the incineration process. In the third phase, ED experiments were carried out during 6 days varying the stirring time (0, 1, 2 and 4 h/day) in order to investigate if energy can be saved on the stirring process. After 6 days of treatment and 4 h/day stirring, 80% and 90% of P was successfully extracted from SSA-A and SSA-B, respectively. This value is very similar to the one obtained for 6 days of treatment stirring 24 h/day.
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Some of the trends and characteristics of the isotopic composition oh precipitation in tropical stations are discussed. Stations in small Pacific islands show a variation with latitude, with lower 8-values between 15°N and 1S°S and higher values at higher. Inland stations are depleted in heavy isotopes with respect to coastal stations but sometimes this continental effect is rather complex, as f,or instance in África. Mean monthly 8-values show a remarkable correlation with the amount of precipitation, but the slope variations do not show a clear dependence on the mean long term 8-value,as should be expected theoretically. In Southern American stations the seasonal variations of the meanmonthly 5-values are correlated and they are greater in inland stations due to con-tinentaly. The possible effects of recycling of water vapour by evapotranspiration are also discussed.
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Fruit tree production is gaining an increasing importance in the central Amazon and elsewhere in the humid tropics, but very little is known about the nutrient dynamics in the soil-plant system. The present study quantified the effects of fertilization and cover cropping with a legume (Pueraria phaseoloides (Roxb.) Benth.) on soil nitrogen (N) dynamics and plant nutrition in a young guarana plantation (Paullinia cupana Kunth. (H.B. and K.) var. sorbilis (Mart.) Ducke) on a highly weathered Xanthic Ferralsol. Large subsoil nitrate (NO3-) accumulation at 0.3-3 m below the guarana plantation indicated N leaching from the topsoil. The NO3- contents to a depth of 2 m were 2.4 times greater between the trees than underneath unfertilized trees (P<0.05). The legume cover crop between the trees increased soil N availability as shown by elevated aerobic N mineralization and lower N immobilization in microbial biomass. The guarana N nutrition and yield did not benefit from the N input by biological fixation of atmospheric N2 by the legume cover (P>0.05). Even without a legume intercrop, large amounts of NO3- were found in the subsoil between unfertilized trees. Subsoil NO3- between the trees could be utilized, however, by fertilized guarana. This can be explained by a more vigorous growth of fertilized trees which had a larger nutrient demand and exploited a larger soil volume. With a legume cover crop, however, more mineral N was available at the topsoil which was leached into the subsoil and consequently accumulated at 0.3-3 m depth. Fertilizer additions of P and K were needed to increase subsoil NO3- use between trees.
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Conflicting opinions are recorded in the literature concerning the suitability of Amazon lands for sustainable agriculture following deforestation. This article has been written to shed light on this question by summarizing climate, landform, soil and vegetation features from the findings of a land resource study of the Brazilian state of Rondônia in south-west Amazonia. The work, which followed the World Soils and Terrain Digital Database (SOTER) methodology, was financed by the World Bank. During the course of the survey special emphasis was given to studying soils; 2914 profiles were analyzed and recorded. The study identified a complex pattern of land units with clear differences in climate, landform, soils and native vegetation. Forested areas mosaic with lesser areas of natural savannas. The latter occur on both poorly-drained and well-drained, albeit nutrient deficient sandy soils. The tallest and most vigorous forests or their remnants were seen growing on well-drained soils formed from nutrient-rich parent materials. Many of these soils could, or are being used for productive agriculture. Soils developed on nutrient-poor parent materials support forests that are significantly lower in height, and would require large lime and fertilizer inputs for agriculture. Low forests with high palm populations and minor areas of wet land savannas cover the poorly drained soils. It is evident that forest clearing in the past was indiscriminant; this cannot be condoned. The diversity of land conditions found throughout Rondônia would suggest that many past studies in the Amazon have simply been too broad to identify significant soil differences.
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As formas orgânicas do nitrogênio em solos são determinadas mediante a identificação e quantificação dos compostos orgânicos liberados, quando os solos são tratados com ácido a alta temperatura. Ainda não se conhecem na literatura trabalhos sobre a natureza química do N orgânico nos solos da Amazônia. O presente trabalho teve como objetivos identificar e quantificar a transformação do nitrogênio proveniente de fertilizantes marcados com 15N nas frações orgânicas nitrogenadas de três solos da Amazônia Central: dois solos de terra firme, classificados como Latossolo Amarelo e Podzólico Vermelho Amarelo e um solo de várzea, classificado como Glei Pouco Húmico. Foram utilizadas amostras de solos de um ensaio de adubação desenvolvido em condições de casa de vegetação, onde, após cultivo, procedeu-se o fracionamento do N orgânico do solo por meio da hidrólise ácida. Foram determinadas as seguintes frações: N-solúvel em ácido e destilado (NSAD), N-solúvel em ácido e não destilado (NSAnD) e N-não hidrolisado (NnH). Nos solos de terra firme, o N orgânico foi encontrado principalmente na forma de N solúvel em ácido e não destilado (NSAnD). Entre 63 a 66% (Latossolo) e 69 a 73% (podzólico) do 15N imobilizado no solo foram encontrados na fração NSAnD. Esses resultados demonstram a importância da imobilização microbiana do N nesses solos. No solo de várzea, ao contrário, houve pouca diferença entre os teores de 15N do fertilizante imobilizado nas frações NSAnD e NSAD. Entre 46 e 53% do total de 15N imobilizado foram encontrados na fração NSAnD, enquanto que 42 a 52% ficaram na fração NSAD. Nesse solo, a presença de argila tipo 2:1 pode ter contribuído para o alto estoque de 15N orgânico incorporado na fração NSAD, devido à fixação de íons NH4+.